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澳大利亚鲨鱼湾高盐海洋环境中现存叠层石的微生物多样性。

Microbial diversity of extant stromatolites in the hypersaline marine environment of Shark Bay, Australia.

作者信息

Burns Brendan P, Goh Falicia, Allen Michelle, Neilan Brett A

机构信息

School of Biotechnology and Biomolecular Sciences, University of New South Wales, Sydney 2052, Australia.

出版信息

Environ Microbiol. 2004 Oct;6(10):1096-101. doi: 10.1111/j.1462-2920.2004.00651.x.

DOI:10.1111/j.1462-2920.2004.00651.x
PMID:15344935
Abstract

Stromatolites have been present on Earth, at various levels of distribution and diversity, for more than 3 billion years. Today, the best examples of stromatolites forming in hypersaline marine environments are in Hamelin Pool at Shark Bay, Western Australia. Despite their evolutionary significance, little is known about their associated microbial communities. Using a polyphasic approach of culture-dependent and culture-independent methods, we report the discovery of a wide range of microorganisms associated with these biosedimentary structures. There are no comparable reports combining these methodologies in the survey of cyanobacteria, bacteria, and archaea in marine stromatolites. The community was characterized by organisms of the cyanobacterial genera Synechococcus, Xenococcus, Microcoleus, Leptolyngbya, Plectonema, Symploca, Cyanothece, Pleurocapsa and Nostoc. We also report the discovery of potentially free-living Prochloron. The other eubacterial isolates and clones clustered into seven phylogenetic groups: OP9, OP10, Marine A group, Proteobacteria, Low G+C Gram-positive, Planctomycetes and Acidobacteria. We also demonstrate the presence of sequences corresponding to members of halophilic archaea of the divisions Euryarchaeota and Crenarchaeota and methanogenic archaea of the order Methanosarcinales. This is the first report of such archaeal diversity from this environment. This study provides a better understanding of the microbial community associated with these living rocks.

摘要

叠层石在地球上已经存在了超过30亿年,分布范围和多样性各不相同。如今,在高盐海洋环境中形成叠层石的最佳实例位于西澳大利亚鲨鱼湾的哈梅林池。尽管它们具有进化意义,但人们对其相关的微生物群落却知之甚少。我们采用依赖培养和不依赖培养的多相方法,报告了与这些生物沉积结构相关的多种微生物的发现。在对海洋叠层石中的蓝细菌、细菌和古细菌进行调查时,尚无将这些方法结合起来的可比报告。该群落的特征是蓝细菌属的生物,包括聚球藻属、异球藻属、微鞘藻属、鞘丝藻属、织线藻属、席藻属、蓝囊藻属、侧孢藻属和念珠藻属。我们还报告了潜在自由生活的原绿藻的发现。其他真细菌分离株和克隆聚集成七个系统发育组:OP9、OP10、海洋A组、变形菌门、低G+C革兰氏阳性菌、浮霉菌门和酸杆菌门。我们还证明了与广古菌门和泉古菌门嗜盐古菌成员以及甲烷八叠球菌目产甲烷古菌相对应的序列的存在。这是关于该环境中古菌多样性的首次报告。这项研究有助于更好地了解与这些活岩石相关的微生物群落。

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